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Atmospheric Limits: A Review of the Effect of Path Length Variations on the Coherence and Accuracy of VLBI

Published online by Cambridge University Press:  03 August 2017

Alan E.E. Rogers*
Affiliation:
Haystack Observatory, Westford, MA 01886

Abstract

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Interferometer phase fluctuations produced by path length variations in the troposphere limit the coherence to between 100 and 1000 seconds at a 3 millimeter wavelength. An expression for the coherence is given using an Allan variance to characterize the atmospheric phase fluctuations. Methods of optimizing the fringe detection threshold and calibrating the fringe visibilities under poor conditions of poor coherence are outlined. The astrometric and geodetic accuracy of VLBI is limited by our ability to calibrate the atmospheric path. Atmospheric “self-calibration” techniques which use the elevation dependence of interferometer delay to solve for the highly variable “wet” component of troposphere are discussed. Various models for the elevation dependence of atmospheric path or “mapping function” are reviewed. The accuracy limits imposed by the atmosphere are discussed.

Type
Instrumentation and Analysis
Copyright
Copyright © Reidel 1988 

References

Armstrong, J.W., and Sramek, R.A., ‘Observations of tropospheric phase scintillations at 5 GHz on vertical paths’, Radio Sci., 17, 15791586, 1982.Google Scholar
Chao, C. C., ‘A model for tropospheric calibration from daily surface and radiosonde balloon measurements.’ Tech. memo Cal. Inst. technol. Jet Propulsion Lab., 391–350, 1972.Google Scholar
Davis, J. L., Herring, T. A., Shapiro, I.I., Rogers, A. E.E., and Elgered, G., ‘Geodesy by radio interferometry: Effects of atmospheric modeling errors on estimates of baseline length’, Radio Sci., 20, 15931607, 1985.CrossRefGoogle Scholar
Hogg, D. C., Guiraud, F. O., and Sweeney, W. B., ‘The short-term temporal spectrum of precipitable water vapor’, Science, 213, 11121113, 1981.CrossRefGoogle ScholarPubMed
Moran, J. M., ‘Very long baseline interferometric observations and data reduction’, in Methods of Experimental Physics, edited by Meeks, M. L., vol. 12, part C., pp. 228260, Academic, New york, 1976.Google Scholar
Marini, J. W., ‘Correction of satellite tracking data for an arbitrary tropospheric profile’, Radio Sci., 7, 223231, 1972. and unpublished note 1974.Google Scholar
Resch, G. M., Hogg, D. E., and Napier, P. J., ‘Radiometeric correction of atmospheric path length fluctuations in interferometric experiments’, Radio Sci., 19, 411422, 1984.Google Scholar
Rogers, A. E.E., Moffet, A. T., Backer, D. C., and Moran, J. M., ‘Coherence limits in VLBI observations at 3-millimeter wavelength’, Radio Sci., 19, 15521560, 1984.Google Scholar
Rogers, A. E.E., and Moran, J. M., ‘Coherence limits for very-long-baseline interferometry’, IEEE Trans. Instrum. Meas., IM-30(4), 283286, 1981.Google Scholar
Rutman, J., ‘Characterization of phase and frequency instabilities in precise frequency sources: Fifteen years in progress’, Proc. IEEE, 66, 10481075, 1978.CrossRefGoogle Scholar
Thompson, M. C., Wood, L. E., James, H. B., Smith, D., ‘Phase and amplitude scintillations in the 10 to 40 GHz band’, IEEE Trans. Antennas Propag., AP-23, 792797, 1975.Google Scholar
Treuhaft, R.N. and Lanyi, G.E., ‘The effect of the dynamic wet troposphere on radio interferometric measurements’, Radio Sci., 22, 251265, 1987.CrossRefGoogle Scholar